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PICTURESQUE 
MEXICO 


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ORB!  S     T  E  R  R  A  R  U  M     SERIES 
Wished: 

Volume    I.  PICTURESQUE  ITALY 

Volume  II  PICTURESQUE  NORTH  AFRICA 

iv.  PICTURESQUE  PALESTINE 

AM)  ARABIA 


PICTURESQUE 

MEXICO 

THE  COUNTRY  •  THE  PEOPLE 
AND  THE  ARCHITECTURE 


JARROLDS   Publishers   LONDON 

Limited,  10  tiinl  11  Warwick  Lane 


>>h  'SJ,  '5s,  l(">>  '7°,  >7>> 
:-'■  24],  245-24-  and  2/2 

.'■!  SeUr-Sc  pis.  2//  and  2\j  by  Teobert 

Museum,  Berlin.     All  the  others  by  Hugo  Brehme,  Mexiko 


Digitized  by  the  Internet  Archive 

in  2011 


1 


http://www.archive.org/details/picturesquemexicOOstau 


Mexico  is  one  of  the  richest  countries  in  the  world.  Nowhere  else  do  we  find 
over  such  an  extensive  area  equallv  favourable  conditions  for  the  formation 
and  enrichment  of  ores.  Nowhere  else  is  there  such  fertility  of  soil  coupled  with 
such  possibilities  of  crop  cultivation  as  in  the  wedge-shaped  southern  end  of  the 
North  American  continent.  The  United  States  of  Mexico  do  not  represent  a 
phvsical  unitv  with  their  two  million  square  kilometres.  The  Isthmus  of  Tehuan- 
tepec  separates  the  States  of  Chiapas,  Tabasco,  Campeche  and  Yucatan  from 
the  northern  part  of  the  countrv.  In  their  geological  structure,  climate,  vege- 
tation and  fauna  thev  belong  to  Central  America. 

The  countrv  to  the  north  of  the  Isthmus  is  chiefly  a  high  plateau.  Along 
the  Rio  Grande  del  Norte  it  is  merelv  the  continuation  of  the  stone  and  waste- 
deserts  of  Arizona  and  New  Mexico  with  their  wide  table-mountains.  To  the 
south  of  the  28 °  latitude  the  grouping  of  the  mountain  ranges  becomes  clearlv 
evident.  The  high  plateau  or  Mesa  Central  is  limited  in  the  west  bv  the  Sierra 
Madre  Occidental  with  its  wealth  of  recent  volcanic  extrusions,  and  in  the  east 
bv  the  folded  chains  of  the  Sierra  Madre  Oriental,  chiefly  built  up  of  limestone 
and  flattening  out  northward  to  the  "Llanos  estacados*'  of  Texas.  Steep  slopes 
deeprv-incised  bv  mountain  torrents,  the  beds  of  which  are  drv  during  most  of 
the  vear,  give  both  of  the  bordering  ranges  a  voting  and  wild  appearance.  In 
its  northern  part,  the  Mesa  Central  is  an  enormous  broad  folded  basin-area 
consisting  of  waste-plains,  without  exterior  drainage,  showing  in  the  Bolson  of 
Mapime  an  altitude  lower  than  a  thousand  metres  above  sea-level.  This  steppe- 
like boundary  district  was  once  the  battle-field  of  nomadic  Indian  tribes  against 
whose  attacks  European  settlers  had  long  to  defend  themselves. 

Between  the  250  and  190  latitude  the  high  plateau  rises  again  to  1,800  and 
2,000  metres,  and  is  divided  up  into  several  broad  and  fertile  valleys,  separated 
bv  ridges  or  timbered  mountain  ranges,  running  as  a  rule  parallel  to  the  edge 
of  the  plateau,  but  in  places  with  a  somewhat  oblique  trend. 

Further  to  the  south  the  countrv  rises  to  the  zone  of  high  volcanos  where 
lava-streams  have  blocked  the  vallevs  in  which,  as  in  the  valley  of  Mexico  and 
further  west  in  the  states  of  Michoacan  and  Jalisco,  great  lakes  were  formed, 
most  of  which  were  salty.  These  parts  of  the  countrv  have  long  been  densely 
populated.  The  strata  of  the  soil  show  the  remains  of  at  least  three  pre- 
Spanish  cultures  superimposed  one  on  the  other:  here  on  the  surface  we  set 
foot  on  historic  ground  full  of  memories  of  recent  Aztec  or  Spanish  times. 
The  highest  volcanoes  are  the  Pic  of  Orizaba  (Citlaltepetl,  Star  Mountain). 
5,594  metres;  Popocatepetl  (the  Smoking  Mountain),  5,452  metres  (which  after 

V 


a  loi  od  of  repose  suddenly  became  active  again  in  1920),  and  Iztaceihuatl 

(the  White  Woman  .  ^.2<S6  metres.  Only  these  volcanoes  are  clad  in  everlasting 

snow.    The  present  snow-line  lies  at  about  4,500  metres     Other  well -known 

inoes  are  the  Nevada  de  Toluca  (XinantecatI)  4. ^  78  metres,  and  in  the 

if  Jalisco,  the  Nevada  deColima(4,378  metres),  with  its  side  cone  thrown 

up  in   1869.    All  these  volcanoes  are  formed  of  andesitic  lava  and  ashes.    A 

volcano  built  up  in  historic  times  is  the  1,700  feet  high  basaltic  cone  of  Mt.Jorullo 

in  the  state  of Michoacan) rising  to  a  height  of  1,820  metres  above  sea  level. 

The  Mesa  Central  ceases  abruptly  south  of  the  volcanic  zone  and  splits  up 
into  a  rugged  low  mountainous  district  deeply  carved  by  the  Rio  Balsas  and 
its  tributaries.    The  greatest  range  in  this  mountainous  district  is  the  Sierra 
Ire  del  Sur,  a  steep  costal  range  sloping  abruptly  into  the  Pacific.   Here  in  the 
surroundings  ofOaxaca  and  in  the  Mixteca  alta,  rocks  of  archaean  age  and  crvsta- 
line  shists  crop  out  over  an  extensive  area.  Boulders  of  archaean  green  stone  may 
have  supplied  the  material  for  the  numerous  little  stone  idols  in  the  Mixteco- 
Tzapotec  style    The  highland  and  the  Sierra  Madre  extend  South  of  the  Isthmus 
from  Chiapas  to  Guatemala.    The  whole  of  the  Chiapas  mountain  region  was 
formerly  the  natural  fortress  of  the  Chiapanecs,  a  warlike  and  very  ancient  Indian 
tribe,    who  maintained  their  independence  against  the  victorious  advance  of 
the  Mexican  rule.    I  Hiring  the  Spanish  rule  Chiapas  belonged  to  Guatemala  as 
the  Provincia  de  San  Vicente  de  Chiapas.    The  descendants  of  kindred  people 
dwell  to  the  south  on  both  sides  of  the  present  state  border.   Here  are  also  the 
inants  of  an  old  superior  Indian  culture  common  to  both  countries. 
Both  the  shores  of  the  Pacific  and   the  Gulf  of  Mexico  are  bordered  by 
narrow  or  broad  coastal  pi  lins.  The  broadest  of  these  belts  is  the  still  uninhabited 
s  steppe  .it  the  lower  part  of  the  Rio  Grande  del  Norte.    This  steppe  is  the 
southern  extension  of  the  P  ostal  plain.    The  peninsula  of  Lower  Cali- 

fornia on  the  Pa<  Ik  .  the  eastern  mountains  of  which  rise  to  i.oo^^  metres,  and 
tin  peninsula  ofYucatan,  on  the  Gulf  of  Mexico,  are  mainly  reached  by  sea  from 
tin-  lest  ot  the  country.  In  their  somewhat  loose  connection  with  the  Mexican 
the)    retain    much    th.it    is    peculiar    to    their    historical    and    economic 
iment 

part  ol  Mi  xtends  south  of  the  Tropic  of  Cancer, 

it  offers  the  most  varied  conditions  tor  vegetation 

It  is  the  elevation  above  sea-level,  and  not 

onl)  latitude  th.it  determines  climate.  There  is  also  it  contrast  between 

and  arid  Pacific   1  0.1st  where  artificial  irrigation  is  even 

m    Onl)  the  Atlantic  winds  bring  rain.  One 

tie  is  the  ( <  intral  p. in  ot  I  ower  <  California  w  here 

ttlements  th<  oases  in  the  places  where 

und  n  dammed  and  collected  behind  artificial  walls. 

i;  in  important  j  ol  the  oil  district,  flows  into  the 

iii«    Rio  Blanco  mu\  Rio  Papaloapam  (along  the 

VI 


banks  of  which  are  vast  sugar-cane  fields),  the  Rio  Coatzacoalcos  and  the 
mighty  streams  Tabascos,  Grijalva  and  Usumasinta.  All  these  rivers  may  be 
navigated  to  the  foot  of  the  mountains  by  ships  of  shallow  draught.  It  is  chiefly 
during  the  rainy  season  in  summer  that  their  turbid  waters  carry  the  mud  of 
the  wild  mountain  torrents  to  the  ocean.  At  their  mouths  they  deposit  broad 
"barras",  the  material  of  which  is  redistributed  along  the  coast  by  the  Gulf 
Stream,  and  accumulated  in  the  form  of  dunes  and  sandy  spits.  The  district 
around  the  mouths  of  the  great  streams  to  the  east  of  the  Isthmus  is  an  alluvial 
plain  of  recent  formation  covered  with  savannas  and  swamps  with  natural 
channels  which  afford  the  only  connection  with  the  interior.  But  on  the  Pacific 
side  the  rivers  break  through  the  mountains  at  the  bottom  of  deep  oak  and 
pine-clad  gorges.  Such  rivers  are  for  instance  the  Rio  Sonora,  Rio  Yaqui  and 
the  powerful  Rio  Grande  de  Santiago  or  Lerma  which  flows  through  the  Lago 
Chapala.  Onlv  the  mouths  of  these  rivers  are  navigable. 

When  we  approach  Mexico  from  Europe  we  only  perceive  the  hot  and  damp 
coastal  strip  of  Campeche,  Tabasco  and  Vera  Cruz  covered  with  a  rank  tropical 
forest  and  sparse -growing  mangroves  along  the  lagoons.  This  is  the  fever- 
haunted  "tierracaliente",  the  home  of  numerous  valuable  timber  trees,dye-woods 
and  tropical  forest  animals.  The  country  towards  the  interior,  Edward  Seler 
tells  us,  consists  of  vast  wooded  plains  with  an  impenetrable  tangle  of  the  most 
varied  deciduous  trees.  Their  foliage  is  shed  irregularly,  and  their  trunks  are 
very  large  with  horizontally  spreading  branches.  In  the  shade  of  these  forest 
giants  the  tree  fern  and  small  palms  thrive,  and  different  sorts  of  bamboo  grow- 
along  the  rivers  and  brooks.  Cocoa  and  rubber-trees  grow  wild  here,  and  the 
vanilla  plant  is  found  climbing  the  trunks  of  various  trees.  The  great  trunks  are 
cumbered  with  innumerable  epiphvtes  or  parasitical  plants  such  as  orchids,araceae, 
ferns  and  bromeliaceae  which  usually  cling  to  the  branches  and  forks  of  the 
branches  and  collect  rain-drops,  humus  and  all  sorts  of  detritus  in  their  funnel- 
shaped  leaves  or  rosettes.  The  cultivation  of  tobacco  in  the  higher  regions  of 
this  zone  dates  from  ancient  Indian  days.  It  is  now  chiefly  grown  in  the  State 
of  Oaxaca  and  in  the  surroundings  of  San  Andres  Tuxtla  in  southern  Vera  Cruz 
on  the  west  foot  of  the  basaltic  group  of  the  San  Martin  volcano.  Towards  the 
steppe,  on  the  outer  fringe  of  the  virgin  forest,  one  often  meets  with  outposts 
of  scattered  groups  of  single  deep-rooted  tropical  trees  such  as  the  tall-stemmed 
silk-cotton  tree  (Bombax  Ceiba  L.J  and  the  shady  fig-tree  (Higo,  Ficus  Am  ate  L.J. 

Great  dryness  is  a  peculiarity  of  the  northern  Yucatan  soil.  Here  the  rain- 
water disappears  in  the  crevices  of  a  young  limestone  mass  forming  a  cover  over 
a  part  of  northern  Yucatan.  The  water  collects  on  an  impermeable  marl  bed 
at  the  base  of  the  limestone  mass  into  subterranean  rivers  and  ponds.  It  is  drawn 
up  through  shafts  ("cenotes"),  and  is  sometimes  bitter.  Now-a-days  it  is  often 
raised  by  means  of  wind-driven  motors.  The  dry  soil  is  particularly  adapted  for 
raising  sisal  hemp  {Agave  sisaleana  or  rigida)  which  gives  this  landscape  its  parti- 
cular character.  Mcrida  is  the  centre  of  the  sisal  hemp  industry. 

VII 


At  a  height  of  between  600  and  1,800  metres,  on  the  slopes  of  the  high 
plateau,  extends  the  "tierra  templada",  the  "temperate  land"",  along  the  Gult 
coast  near  Orizaba  and  Jalapa.  It  is  covered  with  evergreen  woods.  Rain  falls 
here  practically  throughout  the  year.  Heavv  dew  refreshes  the  plants  every  night, 
hut  the  climate,  away  from  the  fever-laden  swamps  of  the  lowland,  is  mild  and 

isant.  Sugar-cane  and  rice  thrive  there  without  artificial  irrigation.  Beside 
,i  large  number  of  indigenous  tropical  fruits  such  as  mammees,  aguacates, 
zapotes,  anonas  and  papaws,  mangos,  oranges  and  bananas,  introduced  from 
the  Mediterranean  and  India,  thrive  here  as  though  thev  were  at  home.  The 
lower  levels  of  this  zone,  as  for  instance  round  Cordoba,  are  often  characterized 
by  red  lateritious  soil  which  glimmers  through  the  green  foliage.  Here  are  the 
c  hief  regions  of  the  cotfee-plant.    In  these  zones,  on  the  southern  slope  of  the 

h  plateau  in  the  State  of  Morelos,  are  situated  the  health-resorts  Cuauthla 
and  (  uernavaca.  The  latter  town  was  presented  bv  Charles  V.  to  the  conqueror 
'  ui us  \\li<>  was  the  tirst  to  cultivate  the  sugar-cane  in  its  surroundings.  Then 
there  is  Oaxaca,  the  capital  of  the  state  of  the  same  name,  and  finally,  on 

south  west  slopes  of  the  plateau,  not  far  from  Guadalajara  (the  second 

st  city   in  Mexico),  all   the  villa  colonies  along  the  shores  of  Lago  de 

Chapala  (the  largest  lake  in  the  country).    The  mountain  region  that  extends 

from   the  elevated   valley   of  Puebla   to  the  coast  of  the  Pacific  was  called 

"mixtlan"  (cloud  land)  bv  the  ancient  Mexican  Indians,  and  is  known  to-day 

a. 

The  tart  that  the  arid  plateau,  the  "tierra  fria"  (cold  land)  is  situated  on  the 

>ide  ol  the  eastern  coast  range,  and  does  not  thus  receive  the  rain  laden 
trade  winds,  explains  its  dry  climate.  (  Inly  about  one  fifth  of  the  precipitation  (A 
the  tierra  templada  of  <  trizaba  tails  here.  The  year  is  divided,  as  further  north 
.mil  along  the  muth  eastern  shore,  into  a  dry  and  rainy  season.  According  to 
I  Seler's  observations  the  months  of  February  to  April  cover  the  period 
ol  1  i  aridity.  The  rain)  season  usually  commences  towards  the 

end  "i  May.   The  maximum  precipitation  and  frequency  o\  thunderstorms  is 

1  from  June  till  July,  and  there  is  a  second  lesser  maximum  in  Septemb 
whereas  ii  1st.  in  the  dog-days,  there  is  usually  a  minimum.  The  thundei 

mostly  in  the  afternoon,  whilst  the  mornings  and  forenoons  are  cl< 
'  time  1  on  the  high  plateau  is  when  the  rain)  season  ends 

in  l  1  lutumn  follows  with  ary,  fresh,  clear  days  ajid  continuall) 

ultivated  plant  of  the  plateau  is  the  maguey 
pi. nit  from  which  pulque  An^l  ixtle  are  made,  and  which  is 

Ids  planted  with  agaves  aic  met  with  far  in  tl  e 

On  thi  f  the  plateau  thick-leaved  opuntias  and  cacti  are  frequently 

ilmsbelon        1    1        rder  liliaceae,  and  thorn-acai 
y  plants  and  ab  ithstand  long  periods  of  drought.  The 

•     odium  trees)  betray  the  preseno 

Mil 


running  or  ground-water.  The  Aztecs  call  them  ahuehuetl,  which  means  "Old 
man  of  the  water". 

Sudden  changes  in  the  landscape  are  only  encountered  in  places  where,  at 
the  edge  of  the  high  plateau  overgrown  with  grass  and  sparse  trees,  the  rivers 
and  brooks  plunge  down  deep  gorges  clad  with  thick  green  foliage.  Sometimes 
the  waterfalls  are  a  hundred  metres  high.  Many  of  them  are  used  to-day  for 
waterpower. 

At  the  time  of  the  diluvial  glaciation  of  northern  America  the  climate  ot  the 
Mesa  Central  must  have  been  cooler  and  at  the  same  time  have  had  a  greater 
precipitation.  Glacial  striae,  cirques,  rochcs  moutonne'es,  snow  and  glacier  deposits 
are  still  to  be  found  on  the  high  volcanoes  about  a  thousand  metres  below  the 
present  snow-line.  Moraines  are  found  as  low  as  3,800  metres  on  the  Nevado 
de  Toluca. 

In  cutting  the  "Canal  del  Desagiie"  about  50  species  of  mammals  belonging 
to  the  different  diluvial  strata  were  found:  the  lowest  stratum  contained  fossilized 
bones  of  a  large  primitive  horse,  the  upper  ones  hyena-like  canidae,  several  felidae, 
the  mammoth -like  elephas  colombi  (spread  all  over  Mexico  in  diluvial  times), 
stags  and  antelopes.  All  these  belonged  mainly  to  a  fauna  of  the  Sonoran  region, 
that  is  to  say  to  the  fauna  of  the  northern  steppes. 

Lateritic  soil  under  the  recent  s.md-blown  deposits,  found  for  instance  in 
San  Luis  Potosi,  suggests  greater  precipitation  in  these  times.  So  too  does  diluvial 
calcareous  tufa,  as  well  as  the  frequent  occurrence  of  lacustre  deposits  in  old 
lake  basins  that  are  now  dry.  Probably  most  of  the  large  caves  in  the  limestone 
mountains  date  from  this  period.  The  remains  on  the  slopes  of  the  mountains 
of  the  once  extensive  forests  of  the  high  plateau  prove  that  the  climate  was 
formerlv  much  moister. 


The  large  northern  border  states  Sonora,  Chihuahua,  Coahuila,  together  with 
Durango  and  Lower  California,  cover  nearly  the  whole  of  present-day  Mexico. 
But  this  bare  northern  district  has  only  a  small  population.  Settlements  are 
chiefly  in  the  mountains  in  connection  with  mines,  along  railways,  and  some- 
times on  the  rivers  along  the  banks  of  which  cotton  is  grown  and  which  flow 
into  the  salt-lakes  ("lagunas")  without  exterior  drainage  of  the  bolsones. 

But  to  the  south  of  Zacatecas  and  San  Luis  Potosi  the  broken  surface  of  the 
country  favoured  the  development  of  smaller  states  at  a  very  early  date.  The  damp 
climate,  which  was  much  more  propitious  to  settlement,  together  with  the  great 
fertility  of  a  volcanic  soil,  favoured  a  greater  density  of  population.  Besides  this 
the  states  of  Hidalgo  and  Mexico  are  the  richest  in  gold.  Hidalgo  is  the  state 
that  produces  the  most  silver.  The  majority  of  the  great  towns  and  cultivated 
areas  are  situated  at  a  height  of  about  1,900  to  2,000  metres.  The  highest  and 

IX 


most  important  valleys  are  those  ofToluca  (2,680  metres).  Mexico  (2. 280  metres) 
and  Puebla  (2,360  metres).   But  agriculture  is  carried  on  as  high  as  3,2 50  metres. 

The  soil  is  very  fertile  where  it  does  not  consist  of  limestone  or  basalt  but 
of  volcanic  tuffs  Maize  and  beans,  the  two  original  food-stuifs  of  the  people,  as 
well  as  wheat  and  barley  (introduced  from  Europe)  grow  annuallv  without 
manuring  and  rotation.  Besides  native  edible  plants  and  fruits  such  as  sweet 
potatoes,  tomatoes  and  capsicums  (the  favourite  spice),  pears,  apples,  peaches, 
apricots  and  tigs  (introduced  from  Europe)  all  thrive  here. 

( )n  the  high  plateau,  the  native  houses  are  built  of  adobe  (sun-dried  bricks  . 
in  contradistinction  to  the  wooded  Gulf  coast  where  the  walls  are  made  of 
bamboo  stems,  whilst  the  steep  roofs  are  covered  with  palm -leaves  or  grass. 
The  ground  plan  of  these  bamboo-huts  is  mostlv  oval  in  the  northern  part  of 
the  Gulf  coast,  or  rectangular  in  the  southern  part.  In  the  villages  the  walls  are 
sometimes  plastered  with  clay  and  whitewashed.  The  ''ranchos*'  often  have 
bakehouses  constructed  of  adobe  or  clay,  sometimes  also  clay  urn-shaped  barns 
for  maize,  standing  on  stone  socles  and  thatched  with  straw.  The  lower  classes, 
especially  the  Indians,  still  live  in  the  same  sort  of  dwellings  as  in  pre- 
( Columbian  time 

The  ancient  cultures  of  Mexico  are  concentrated  on  the  high  plateau  in  the 

on  south  of  the  Tropic  of  Cancer  on  the  border  towards  the  steppe,  just  as 
the  pre  Incan  culture  attained  to  its  highest  development  and  Incan  culture 

lied  its  greatest  power  of  expansion  on  the  highland  of  Peru  and  Bolivia  in 
the  southern  border  district  of  the  tropical  zone  towards  the  Puna.  The  cultures 
<>|  ancient  Mexico  attained  to  the  highest  development  in  the  northern  bordering 
climates  Probably  man  has  long  lived  in  this  part  as  a  hunter  and  made  use 
of  tire  and  neolithic  weapons  and  implements. 

Following   a    most    ancient    culture    with    earthenware    figures  oi  a    very 

primitive   style     productions  of  the   (  )tomi   Indians  and  kindred   tribes),   we 

find   to  the  north  of  the  present  capital  the  development  of  a  first  archaic  art 

of  .1  ven  original  culture  (perhaps  never  superseded  in  later  times)  and  whose 

founders  were  the  Toltecs,  a  Nahua  tribe  surrounded  with  mythical  legends  And 

«  oming  from  the  north.  The  existence  of  the  flourishing  empire  of  Tollan,  erected 

1  >iK  t/.iL  ouatl,w  ho  was  both  priest  and  king,  isproved  bythe  ruins  in  Tula, 

i  reotihuacan  and  other  places  Earthenware  vessels  and  figures 

oft':  tihuacan  typ<         found  neai  Azcapotzalco,  San  Miguel  Amanda  and 

oth(  illey  of  Mexico;  further  at  Puebla,  Tlaxcala,  Pdnuco,etc. 

Thus  \\(    m.i\   presume  that  the  (  ulture  of  this  ancient  empire  (Mice  included  the 

•  in  .in  .1  of  the  high  plateau  ami  a  large  part  of  the  neighbouring 

influence  in  these  parts  According 
to  Fray  B  rLehmann  tells  us,  the  ancient  Toltec 

;  ml  of  th(  1  nlui\  A  I  y  The  (  >lm< 

the  downfall.    But  ancient  Toltec  culture 
with  Cholula  as  the  centre  and  trading  city.   Teotihuacan 


and  Tollan,  however,  and  probablv  Cholula,  were  already  ruins  when  the  Spa- 
niards arrived.  In  the  i  i th  century  A.  D.  the  Young -Toltecs  emigrated  under 
the  leadership  of  Quetzalcouatl  -  ee  Acatl  to  the  countries  of  the  Atlantic  and 
Pacific  coasts,  to  Tabasco  and  Soconusco.  Mention  is  made  in  documents  that 
the  voung  Toltec  dispersal  had  been  hastened  by  famine;  a  phenomenon  that 
is  not  unusual  in  climatic  border-lands. 

According  to  Walter  Lehmann  the  calendar  of  the  old  Toltecs  was  based 
on  a  lunar  "Weltanschauung",  whereas  Cholula  became  the  intellectual  centre 
of  a  reform  of  the  old  religious  system,  and  the  sun  was  the  centre  of  their 
•Weltanschauung".  This  found  its  expression  in  the  reform  of  the  calendar. 

Mexican  culture  had  spread  in  successive  waves  from  the  high  plateau  districts 
to  the  lowlands.  Thus  we  find  names  of  villages  and  ranchos  in  an  ancient 
Nahua  dialect  in  the  district  of  the  Rio  Panuco.  For  instance,  the  Pipils  of 
Guatemala  and  Salvador  and  the  now  extinct  Nicarao  of  Nicaragua,  who  spoke 
ancient  Nahua  dialects,  are  descendants  of  the  Toltecs.  It  becomes  evident  that 
during  these  migrations  older  pre-Mexican  tribes  were  partly  scattered  and  partly 
squeezed  into  enclaves.  This  explains  the  patchwork  appearance  of  the  peoples 
and  fractions  of  peoples  which  strikes  us  when  looking  at  a  map  of  languages  still 
spoken  in  Mexico. 

It  is  possible  that,  contemporaneously  with  the  flourishing  period  of  older 
cultures  on  the  Mexican  plateau,  the  old  Maya  peoples,  who  had  long  been  living 
round  the  border-district  of  Chiapas  and  Guatemala,  developed  at  the  same  time. 
Palenque,  Ococingo,  Piedres  Negras,  Menche,  Tikal,  Quirigua  and  Copan  were 
ancient  cities  here,  and  with  the  exception  of  the  first  two,  were  all  situated  in 
Guatemala  and  Honduras.  Of  these  cities  Palenque  is  said  to  be  the  first  to  have 
been  abandoned.  On  the  arrival  of  the  Spaniards  all  these  once  so  nourishing 
settlements  belonged  already  to  the  past. 

The  Mava  culture  also  had  its  renaissance,  as  for  instance,  within  the 
confines  of  the  Yucatan  peninsula  where  there  is  one  set  of  ruins  next  to  the 
other,  and  where  ancient  American  architecture  reached  the  zenith  of  its 
development.  Known  places  here  are  Uxmal,  Kabah,  Labna,  Sayi,  Tulum  and 
Akanceh.  There  is  a  report  that  in  the  pre-Spanish  epoch  Nahuas  (Itza)  had 
penetrated  into  Yucatan  under  a  leader  named  Kukulcan  (Quetzalcouatl). 
Cities  like  Chicffen  Itza  and  Mayapan  may  be  considered  as  mainly  Toltecan 
settlements  both  according  to  tradition  and  archaeological  discoveries.  The 
Quetzalcouatl  facades  of  the  Yucatan  edifices,  the  Chich'en  Itza  feather-snake 
columns  and  the  strange  semi-recumbent  Chaac-Mol  figures  (libation  vessels) 
point  emphatically  to  Toltecan  influence.  History  tells  us  further  that  Mayapan 
was  destroyed  (circa  1450  A.  D.)  by  a  Maya  rising.  After  the  destruction  of 
Mayapan  the  old  Indian  culture  of  Yucatan  decayed,  and  where  once  numerous 
large  cities  and  mutually  united  principalities  flourished,  the  Spanish  conquerors 
only  found  small  communities  at  war  with  each  other. 

All  these  ancient  cultures  cannot  be  conceived  without  agriculture,  the  basis 

XI 


of  which  throughout  the  whole  of  Mexi  o  was  the  cultivation  of  maize.  The 
wild  original  maize- plant  (Euchlaena  luxurians),  known  as  teosinte,  is  native  to 
the  Pacific  coast  of  Guatemala.  Whereas  a  group  of  plants  such  as  manioc  are 
characteristic  of  the  damp  Atlantic  virgin-forest  districts  of  America,  maize,  in 
spite  <>f  its  adaptability,  is  chiefly  confined  to  the  dry  and  higher  parts  of  Mexico. 
Nowadays  the  two  states  of  Jalisco  and  Zacatecas  supply  half  the  annual  maize 
crops.  In  Mexico  and  Central  America  the  growth  of  the  ancient  state  and  its 
development  to  a  really  high  culture  is  limited  to  the  arid  districts  where  maize 
is  ( ultivated 

In  the  old  times  it  was  chiefly  the  temples  that  were  built  of  stone.  An 
elevated  position  was  preferred  for  sacred  spots  and  the  buildings  belonging  to 
them.  Thus  one  found  on  the  Gulf  coast  in  the  Huaxteca  country  roughlv  hewn 
stone  sculptures  of  which  some  may  have  stood  in  the  wooden  sanctuaries  as 
well  as  in  important  parts  of  the  settlements  on  artificial  earth  mounds  which 
were  only  surrounded  by  walls  where  suitable  stone  slabs  were  ready  at  hand. 
But  on  the  Mexican  high  plateau,  as  well  as  in  Chiapas,  Guatemala  and  Yucatan 
the  stone  eella  like  sanctuaries  or  other  temple  buildings  rose  from  the  platforms 
of  step  pyramids.  Other  edifices  were  on  terrace-like  substructures  of  which  many 
were  orientated  so  as  to  coincide  with  the  cardinal  points.  These  step-pyramids 
erected  over  stone  heaps  and  earth  mounds  stood  in  roomy  courtyards  with 
numerous  out  buildings  and  were  often  of  huge  dimensions.  In  front  of  the  main 
temple  in  Mexico  City  there  was  King  Tizoc's  ("Tlacktemalacatl")  great  sacri- 
ficial stone.  The  sacrificial  receptacle  ("quauhxicalli")  to  catch  the  blood  of  the 
sacrifice  also  belonged  to  the  ceremonial  vessels.  Within  the  Mexican  temple 
grounds  is  also  the  sacred  ball-court  ("tlachtl")  dedicated  to  the  gods    How- 

:.  such  a  court  is  lacking  in  Teotihuacan,  but  there  is  one.  for  instance,  in 
Chich'en  lt/.i  The  ball  game,  in  which  a  rubber  ball  ("olli'^was  used. was  much 
in  vogue  in  the  sphere  ol  Mexican  culture  and  was  played  by  the  people. 

Vmong  the  gigantic  ruins  ol  Teotihuacan.  the  two  stone  cased  mounds  known 
•is  tin   "P.!<   m"  and  ••Sun"  pyramids  are  particularly  conspicuous,  whilst  quite 
Quetzalcouatl  temple  with  rich  sculptures  was  freed  from  its  v< 
:  debris  in  thi  llled  "Ciudadela"  situated  (Mi  the  southern  side  o\ 

the  Rio  San  Juan 

The  pyramid  ol  Cholula  covers  the  greatest  area.  To-day  a  church  dating 
olonial  period  stands  on  its  crest    An  ancient  trade  route  led 

Cholula,  the  celebrated  centre  ol  the  Quetzalcouatl  cult,  and  also  that  o\ 

trade,  and  famous  '  ellent  ceramics  and  other  products  of  flourishing  arts 

and  rhis  route  extende  !  to  anahu  on  the  Boca  de  TeYminos 

ol  the  Maya  district)  and  to  anahu        yotlan  the  coastal  snip 

hi<  h  is  i  foi   its  co(  oa  tree  plantations.     The 

neai  <  uernavaca  differs  from  those  on  the  high  plateau 

•in  A.w  symbols  and  the  employment  ol  a  line 

'I  ol  i  as  was  especiall)  the  custom  on  Maya  monuments 

Ml 


of  a  certain  period).  The  pyramids  in  theTzapotec  country,  as  for  instance  those 
crowning  a  hill  300  metres  high  at  the  foot  of  Monte  Alban,  and  the  edifices  of 
Mitla  near  Oaxaca,  famous  for  their  mosaics,  frescos  and  columns  belong  to  the 
pre-Aztec  period.  The  pyramid  of  ElTajin  nearPapantla  in  theTotanac  region  in 
the  State  of  Vera  Cruz,  the  steps  of  which  are  interrupted  by  numerous  niches, 
is  also  pre-Aztec.  The  pyramid  of  Huexotla  (Hidalgo),  Castillo  de  Teavo  (Vera 
Cruz)  and  the  pyramid  ofTepozlan  (D.  F.)  which  stands  high  on  a  hill  over  the 
present  town  may  be  mentioned  as  examples  of  Aztec  temple  pyramids  in  small 
provincial  towns. 

The  edifices  of  the  Maya  in  Yucatan  were  technically  the  most  perfect.  It 
was  here  that  the  sacrarium  was  further  developed.  It  contained  two  long  corridor- 
like spaces  which  were  covered  with  a  sort  of  vaulting  constructed  of  layers  of 
steep  stone  slabs  each  projecting  over  the  other.  "The  front  corridor  opens  onto 
a  columned  gallery  towards  the  steps,  the  back  corridor  contains  a  special  small 
cella  with  the  idols.  The  upper  vertical  facade  is  decorated  with  rich  "Baroque" 
ornaments  cut  in  limestone  blocks  with  fantastic  masks  of  gods  "  (W.  Krickeberg.) 

The  Aztecs  or,  in  the  narrower  sense  of  the  word,  the  Mexicans  (the  Mexica) 
were  the  heirs  of  Toltec  culture  on  the  Mexican  high  plateau.  Thev  traced  their 
origin,  especially  the  inhabitants  of  Tetzcoco,  from  the  Chichimecs.  The  Aztecs 
traced  their  name  back  to  a  legendary  home  ("aztlan").  Like  the  Toltccs  thev 
had  migrated  from  the  north.  From  a  philological  point  of  view  the  Nahuatl- 
speaking  Aztecs  (belonging  to  the  group  of  the  Nahuatlacan-speaking  tribes),  as 
well  as  the  Nahuat-speaking  Toltecs  belong  to  the  Sonoran  linguistic  stock  who 
spread  far  to  the  north-west  and  across  the  frontier  of  Mexico.  According  to 
traditions  the  foundation  of  Mexico-Tenochtitlan  dates  back  to  the  vear  1 3  2  5  A.  D. 
But  in  ancient  times  Colhuacan  was  the  metropolis  of  Mexico-Tenochtitlan. 

The  view  of  this  city  must  have  been  beautiful  bevond  description,  situated 
as  it  was  in  the  salt-lake  of  Tetzcoco.  Like  Venice  it  was  intersected  bv  numerous 
canals  and  built  on  dams  and  sand-islands  surrounded  bv  wooden  piles.  Where 
the  cathedral  now  stands  the  step-pvramid  rose  in  five  steep  terraces.  Its  base 
was  square;  its  sides  are  said  to  have  had  a  length  of  375  feet.  It  was  only  built 
in  1487.  It  contained  a  cella  for  each  of  the  two  gods  Uitzilopochtli  (the  real 
Aztec  national  or  war-god)  and  for  the  rain-god  Tlaloc.  The  king  and  princes 
lived  in  extensive  palaces.  The  life  of  the  people  was  chiefly  concentrated  in  the 
market  near  the  main  temple.  It  is  said  that  when  Cortes  entered  the  citv  en 
the  8th  of  November  15 19  A.  D.  the  inhabitants  numbered  300,000.  That  is 
about  one-third  of  the  present  population. 

In  some  respects  the  Aztec  state  was  a  military  monarchy  with  extensive 
organizations  of  political  and  religious  bodies.  But  even  the  high  valley  of  Mexico 
was  not  a  unified  state.  There  were  three  leading  principalities:  Tenochtitlan, 
Tetzcoco  and  Tlacopan  which  were  held  together  bv  an  offensive  and  defensive 
alliance,  in  which,  however,  Tenochtitlan  predominated.  The  neighbouring 
Tlaxcala  was  a  free  state.    The  important  nation  of  the  Tarascans,  an  ancient 

XIII 


tribe  with  a  distinct  language  and  inhabiting  Michoacan  far  to  the  west,  had 
remained  independent  of  Aztec  rule.  The  advance  of  Cortes,  only  successful 
because  of  the  help  of  the  Totonacs  and  Tlaxcaltecs,  shows  us  how  the  different 
tribes  quarrelled.  But  in  contradistinction  to  the  conditions  in  Yucatan,  the 
Aztec  empire,  which  was  hardly  two  centuries  old,  was  at  the  time  of  the  Spanish 
conquest  still  in  full  possession  of  its  power,  although  governed  by  Montezuma  II, 
(Motecuzoma) an  irresolute  and  melancholv  monarch.  Under  the  powerful  rulers 
of  ancient  times,  especially  of  Motecuzoma  I.  and  his  successors,  many  cities 
and  districts  belonging  to  numerous  neighbouring  tribes  were  successfully  sub- 

i ted  bv  the  Aztecs.  Of  this  we  have  information,  especially  from  trie  im- 
portant hieroglyphics  in  the  Codex  Mendoza,  both  as  to  the  conquests  and  impor- 
tant cultural  tributes.  About  50  years  before  the  arrival  of  Cortes,  the  Aztec 
empire  had  extended  to  the  Gulf  of  Mexico.  The  subjugated  countries  were  not 
incorporated,  but  fortresses  and  garrisons  were  established  to  levy  tribute.  The 
destruction  of  so  many  antiquities  and  cultural  monuments  in  the  Totonac 
district  of  Vera  Cruz,  as  well  as  the  replacing  of  ancient  place-names  bv  Aztec 
designations  bear  eloquent  witness  to  the  methods  employed  bv  these  conquerors. 

According  to  Walter  Lehmann  the  Aztec  language  was  equal  to  all  the 
requirements  of  a  powerful  empire  in  contradistinction  to  the  manv  other  pho- 
netic -ally  and  grammatically  complicated  Indian  languages.  For  manv  years  Aztec 
also  served  as  the  official  language  during  the  Spanish  colonial  period. 

To  the  south  of  the  capital,  on  the  fresh-water  lake  of  Xochimileo.  Aztec 
gardens  are  still  extant  which  arc  called  bv  the  misnomer  "swimming  gardens". 
The  very  fertile  black  soil  was  drained  by  canals  of  various  width  and  the  \c 
table  plots  enclosed  by  stakes  and  trellis  work.   Such  enclosed  plots  were  called 
"chinampas". 

If  we  enquire  what  was  the  chief  difference  between  ancient  American  and 
European  culture  we  shall  find  that  iron,  domestic  animals  (with  the  exception 
<>t  the  turkey),  vehicles,  wheels,  the  potter's  wheel  and  firearms  were  unknown. 
In  architecture  the  vaulted  arch  was  also  unknown.  Cold  and  silver  were 
employed,  .is  well  as  copper;  the  latter  partly  for  bronze.  The  land  was  cleared 
and  stone  was  hew  11  with  stone  or  metal  implements.  The  Huaxtecans  and 
I  "ton. i,  s  on  the  Gull  ol  Mexico  cultivated  cotton  and  wove  fine  shawls  and 
garments  ol  it  Particularly  in  Tabasco,  but  also  on  the  Mexican  high  plateau. 
fine  work  was  executed  in  birds  leathers.    The  Olmecs  on  the  Atlantic 

1  to  the  south  ol  Vera  <  juz  derived  their  name  from  caoutchouc  (ollij  w  hich 

the\  employed  foi  various  purposes.     Milk,   butter  and  cheese  wire  unknown 

I  i  instead  ol  sugar,  and  bee  keeping  is  still  extensively 

carried  on  in  1         untry.   The  use  and  development  oi  hieroglyphics  and  the 

■  lopmeni  ol  the  1  alendar  system  raised  the  Mexican  ( Central  American  sphere 

ultUH  •      •        the  Other  advanced  Amerinds. 

onl)  sun  c  the  Spanish  colonization  that  European  domestic  animals 
ntrodu  .11  the  horse,  horned  cattle,  sheep  and  goats,    The 

XIV 


Spaniards  were  the  first  to  mine  silver,  mostly  by  surface-mining.  The  hammock, 
which  is  now  so  largely  used  in  Yucatan  and  the  Isthmus,  is  said  to  have  been 
introduced  by  the  Spaniards  into  Mexico  from  South  America  via  the  Antilles. 
History  in  America  as  written  in  Europe  is  only  met  with  since  the  beginning 
of  the  1 6th  century. 

i    -5 

The  Roman  Catholic  Church  set  foot  in  Mexico  with  the  Spanish  conquerors. 
Franciscan  monks  were  the  first  teachers,  the  first  historians  and  the  first  pro- 
tectors of  the  ill-treated  unfortunate  natives.  The  number  of  Spanish  Baroque 
churches,  chapels,  monasteries,  schools,  noblemen's  seats  and  buildings  on 
Spanish  haciendas  was  very  great.  The  aqueducts  with  their  towers  and  bridges 
are  striking.  Handicrafts  tlourished  in  the  cities  where  each  had  its  own  quarters. 
According  to  historical  records  a  German,  a  pupil  of  Gutenberg,  is  said  to  have 
introduced  the  art  of  printing  into  Spanish  Mexico  and  also  to  have  published 
a  newspaper. 

The  oldest  church  is  in  Tlaxcala.  It  dates  from  the  year  1 521.  The  church 
of  Titzatlan  near  Tlaxcala  is  also  very  old,  and  unique  in  its  restrained  Renais- 
sance style.  The  atrium  of  the  cathedral  in  the  capital  dates  from  the  year  1525. 
The  main  facade  was  only  completed  in  1667.  The  greatest  of  the  Mexican 
churches  visited  by  pilgrims  was  erected  in  1532  in  Guadeloupe  Hidalgo  near 
the  steep  rock  of  "Tepeyacac".  The  city  of  Puebla,  which  for  many  centuries 
was  to  be  the  trading  centre  between  Spain  and  Mexico,  was  founded  in  the 
same  year.  It  is  the  town  with  the  most  churches,  and  where  the  art  of  making 
glazed  tiles  ("azulejos"),  introduced  from  Spain,  developed.  The  ecclesiastical 
and  secular  subjugation  of  the  north  from  Mexico  to  California  and  of  the  coastal 
strip  on  the  Gulf  of  Mexico  proceeded  from  the  capital  and  the  high  plateau. 
One  of  the  oldest  churches  in  the  Mexican  Gulf  region,  built  in  1749,  is  in 
Altamira,  north  of  Tampico,  a  place  from  which  a  long-established  salt  trade 
was  carried  on  up  the  Rio  Panuco,  and  southwards  to  the  Huaxteca  by  the 
Huaxtec  Indians. 

Five  governors  and  sixty-two  vicerovs  have  ruled  Mexico.  It  is  characteristic 
of  these  times  that  about  a  third  of  the  silver  circulating  in  Europe  in  the  18th 
and  1 9th  centuries  came  from  Mexican  mines.  Spanish  rule  lasted  three  centuries. 
During  the  last  years  of  its  decline,  Alexander  von  Humboldt  visited  Mexico 
(1803/4).  This  was  an  epoch-making  journey,  and  it  is  remarkable  that  no  diaries  of 
the  great  German  explorer  are  known  of  this  journey.  Dissension  in  connection 
with  the  Spanish  succession  and  the  example  of  the  secession  of  the  United 
States  from  England  led  in  1 8 1  o  to  the  outbreak  of  the  struggle  for  indepen- 
dence. The  idea  was  favoured  bv  the  Vicerov  himself,  but  it  had  its  roots 
in  the  people.  Miguel  Hidalgo  v  Costilla,  who  was  57  at  the  time,  and  curate  of 
the  village  Dolores  in  Guanajuato,  became  the  leader  of  the  movement  and  rang 

XV 


the  bells  as  a  signal  of  revolt  on  the  night  of  i  s,h  September  and  placed  himself 
at  the  head  of  the  movement.  The  idea  of  freedom,  which  was  also  enthusiastic- 
allv  greeted  by  the  Indians,  was  never  given  up.  Hidalgo  himself,  however,  had  to 
retreat  before  the  superior  forces  of  Spanish  troops  and  was  captured  and  shot 
in  i  <S  i  i ,  after  numerous  battles,  together  with  the  priest  Morelos.  In  1820 
General  Iturbide  put  himself  at  the  head  of  the  revolutionarv  movement.  He  first 
Jit  on  the  side  of  Spain  and  then  on  that  of  the  revolutionaries  and  pro- 
claimed the  independence  of  Mexico  in  1821. 

Violent  political  struggles  kept  the  country  in  a  turmoil,  and  in  addition  to 
the  internal  troubles  war  broke  out  with  the  United  States  which  ended  with 
the  loss  of  Texas  (1845)  and  California  and  New  Mexico  (1846).  In  1848  the 
Rio  Grande  del  Norte  was  established  as  the  northern  frontier  of  Mexico.  The 
gifted  Benito  Juarez,  a  man  of  indomitable  energy,  born  as  a  poor  Indian  in  a 
little  village  in  Oaxaca,  stepped  to  the  front.  He  was  victorious  in  the  armed 
stnu  _ainst  the  church  ( 1855 — 61),  reformed  the  laws  and  finallv  survived 
as  president  of  the  Republic  the  disastrous  intervention  of  Napoleon  III.  who, 

ther  with  Maximilian  of  Austria,  wanted  to  erect  a  Mexican  empire  in  1867. 
Numerous  urban  gardens  and  decorations  in  the  castle  of  Chapultepec,  the  roval 
seat  of  Mexico,  date  from  this  French  period. 

Benito  Juarez  died  in  1872.  New  troubles  arose.  Thev  were  put  an  end 
to  by  Genera]  Porfirio  Diaz,  Mexico's  greatest  statesman,  who  had  alreadv  re- 
taken the  capital  from  the  French  in  1867,  and  who  became  president  in  1877. 
He  is  the  real  originator  of  the  social  and  economic  reforms  and  public  education. 

I  Hiring  the  thirty-three  years  of  peace  under  this  both  intellectuallv  and  morally 
eminent  man  economic  conditions  reached  their  highest  development.  The  invest 
ment  of  European  capital,  especially  Fnglish  and,  later  on,  American  gradually 
iik  reased.  The  extension  of  the  railway  svstem  took  place  during  the  years 
1  to  [910,  as  well  as  the  completion  of  several  harbour  works,  namely 
those  ..I  the  town  of  Vera  Cruz  which  was  formerly  protected  from  attacks  by 

by  the  fortress  of  San  Juan  de  Ulua. 

Numerous  modern  public  and  private  buildings  in  the  capital,  .is  well  as  in 

.ill  the  cities  o|  Mexico,  were  erected  in  this  period,  and  further  the  new  quarters 

such  .is  Colonia  Roma  and  Juarez  in  the  capital  and  the  garden  cities.    The 

•    i  sanitary  works  ami  draining  of  the  capital  were  finally  completed 

in  1900  undei  Porfirio  Diaz  by  the  construction  of  the  "Canal  del  Desague", 

which  is  thirty  miles  long,  .is  well  ;is  the  "Tunel  tic  Tequixquiac".    In  \<)oo 

M(  •  it)  I). id    51  1  inhabitants.    To-day  with  over  \.oooamh)  souls,  it  is 

the  !  "I  .ill  highland  towns  <>t  the  new  world,  being  situated  at  an  altitude 

m<  to  s  abo>  level 

I  he  grand  tens  in  celebration  of  Mexican  independence  in  1910  marked 

the  ni'  .1  in  Porfirio  Diaz'  term  of  office.    The  same  year  saw 

the  sudden  end  ol  tins  .  real  period  of  development.  With  the  Madero  and  later 

'    irranza  revolutions  in  the  north  began  a  period  of  1^  years  of  intense 

Ml 


unrest  and  social  upheavals  which  were  onlv  possible  in  times  of  violent 
dissension  and  war  between  the  European  peoples  themselves.  During  these 
vears  of  heavy  losses  of  foreign  capital  and  of  the  growing  influence  of  the 
United  States  onlv  the  oil  districts  on  the  Gulf  coast,  the  centre  of  which  is 
Tampico,  were  economically  prosperous.  This  period  of  prosperity  started  at 
the  end  of  1910  with  the  bringing  up  of  the  two  gushers  Potrero  del  Llano 
No.  4  (belonging  to  W.  D.  Pearson  the  constructor  of  the  harbour-works  on 
the  Gulf  coast)  and  Juan  Gasiano  Nos.  6  and  7  (belonging  to  the  American 
E.  L.  Dohenv)  which  suddenly  established  Mexico's  reputation  as  an  oil  coun- 
try. To-day  petroleum  is  by  far  the  most  important  item  in  the  revenues  of 
the  state. 

In  19 1 7  the  new  constitution  came  into  force  under  President  Carranza, 
whose  merit  it  was  to  have  kept  Mexico  politically  neutral  during  the  GreatWar. 

Mexico's  favour  is  much  sought  after  as  a  supplier  of  raw  material.  This 
country  with,  it  is  said,  a  population  to-dav  of  1 5  /.  million  inhabitants  holds 
the  first  place  in  the  production  of  silver,  the  second  in  oil  and  lead,  the  fourth 
in  gold  and  the  fifth  in  copper.  Other  metals  exported  are:  zinc,  mercury, 
arsenic,  antimony,  molybdenum  and  tin.  Other  exports,  besides  petroleum,  are 
graphite  and  semi- precious  stones.  Mexico  has  no  coal.  But  there  is  enough 
lignite,  iron  and  waterpower  for  home  consumption.  The  chief  agricultural 
exports  are  cotton,  sisal  hemp,  tobacco,  sugar,  coffee,  cocoa,  vanilla,  precious 
woods  and  dve-woods  and  tropical  fruits.  As  home  industry  is  not  much  deve- 
loped, finished  goods  are  chiefly  imported. 

Mexico's  great  wealth  is  intimately  connected  with  the  geological  structure 
of  the  country.  Most  of  the  mountain  ranges  are  built  up  of  a  thick  series  of 
folded  limestone  banks  intruded  in  the  period  of  mountain-building  bv  mag- 
matic  rocks  which  brought  up  the  ores  from  the  bowels  o\  the  earth.  Laccolithes 
(of  diorites  and  svenites)  and  dome-shaped  masses  (of  porphvriesi.  in  the  contact 
zones  of  which  the  most  copper  ores  are  found,  form  the  nuclei  of  the  anticlines 
and  folds.  On  the  southern  and  western  part  of  the  Mexican  High  Plateau, 
the  older  eruptive  rocks,  the  andesites,  are  especially  met  with  as  pipe-fillings  and 
lavas.  The  gold  and  silver  ores  are  connected  with  these  older  effusive  rocks. 
The  greatest  ore-vein,  near  Pachuca.  is  16  kilometres  long,  and  the  most  exten- 
sive silver-lode,  the  Beta  Madre  of  Guanajuato,  often  1 50  metres  wide,  is  many 
kilometres  long.  Under  the  silver-bearing  rocks,  in  deeper  zones,  veins  of  galena 
and  zincblend  occur.  Thev  are  also  spread  over  the  limestone  mass  even  some 
distance  from  the  intrusive  body.  In  the  tertiary  period,  on  the  western  side 
of  the  high  plateau,  especially  in  the  Sierra  Madre  Occidental,  streams  of  fresh 
volcanic  lava  poured  out  again  and  again  along  the  fractures  and  faults  over  the 
already  eroded  and  buried  folded  limestone  ranges.  The  obsidian,  of  which  the 
Indians  made  their  skilfully  shaped  sacrificial  knives,  spears  and  arrow-heads,  is 
a  glassv  species  of  this  most  acid  of  lavas.  Where  in  the  most  recent  geological 
epoch  effusive  activity  was  limited  to  single  areas,  such  as  on  the  southern  edge 

XVII 


of  the  high  plateau,  great  crater  volcanoes  were  thrown  up.  Hot  mineral 
springs  are  the  last  traces  of  this  volcanism  on  the  high  plateau.  Both  on  the 
Atlantic  and  Pacific  coast  effussive  rocks  are  basalts.  The  famous  oil-pools  of 
the  oil-fields  north  and  south  of  the  Panuco  River  vallev  are  secondarv  accu- 
mulations of  the  precious  liquid  in  cavities  of  the  limestone  banks  which  are 
closelv  shut  off  from  the  surface  bv  a  gentlv  folded  series  of  impermeable  marls. 
The  limestone  masses  are  also  excellent  water  reservoirs.  Numerous  fresh-water 
springs  How  from  the  rock  at  the  foot  of  the  Sierra  Madre  Oriental.  Where 
there  is  gypsum  in  deeper  parts  of  the  limestone  series,  the  water  comes  up  as 
a  sulphur  spring. 

On  Mexican  soil  the  folded  North  American  mountain-ranges,  which  origi- 
nated somewhat  earlier  towards  the  end  of  the  cretaceous  period,  are  replaced 
I  \  the  ( Central  American  arcs  thrown  up  in  the  tertiary  period.  The  shape  and 
contour  of  the  Mexican  land  mass  resulted  from  the  interaction  of  these  different 
mountain-building  movements.  The  uplift  of  the  Mesa  Central  is  a  consequence 
of  this  crucial  folding,  and  is  the  cause  of  the  tempering  of  the  tropical  climate. 

Dr.  Walther  Staub 


W  III 


INDEX   OF  NAMES  AND   PLACES 


Acambaro   186 

Acatepec  134 

Ajusco  99 

Amecameca  101,  104—113,  120 

Antigua  (Vera  Cruz)  6,  7 

Archeological  photographs  22, 
42—53,  138,  154-157,  172, 
173,  242,  243,  248—253 

Atlixco  137 

Atoyac  8—11 

Cacahuamilpa  (Guerrero)    168, 

169 
Campeche  254—256 
CastillodeTeayo(VeraCruz)242 
Chalchicomula  20,  21 
Chapultepec  38,  40,  41 
Chich'enitza  (Yucatan)  248     250 
Chihuahua  228,  229 
Cholula  138,  139 
Churubusco  64,  65 
Cihuapam  (Vera  Cruz)  247 
Colima  178,  179 
Cuernavaca  162 — 166 
Cuicatlan   143 

Desierto  de  los  Leones  69 — 71 

Guadalajara  188 
■Guadelupe  Hidalgo  26,  30,  31 
Guanajuato  218,  219 
Guayamas  (Scmora)  210 
Guerrero  177 
Guiaroo  near  Mitla  156 

Huaxteca  Indian  (Vera  Cruz)  238 
Huixquilucan   103 

Jalapa  13 

Isla  de  las  Mugereb  (Yucatan)  251 
Juanacatlan  182 
Ixtacalco  78 

Iztaccihuatl  98,  105,  109,  113, 
114,  117,  119,  121-127 


.,  -  -  ■ ,  »"•-') 


Kivic  (Yucatan)  253 


La  Caldera  96,  97 

La  Canada  D  F.  72,  73 

Laguna  del  Carmen  2 

Lake  Chapala   190-195 

Las  Canoas  231 

Los  Remedios  54,  55 

Lower  California  209 

Magdalena  (Sonora)  208 

Manzanillo  207 

Mazatlan  204—206 

Mexico  City    27-29,32  —  38, 

40—45 
Mirador  232 
Mitla  154-157 
Mixteca  alta   145 
Morelia  187,  189 

National  Park  69—71 
Necaxa  (Puebla)  244 
Nonoalco  66 

Oaxaca   144,  146—153 
Ocotlan   183 
Ometusco  100 
Orizaba   14 
Ozumba  102 

Panuco  River  239 
Patzcuaro  196—201 
Peak  of  Orizaba   1,  16-19 
Popocatepetl  98,  104,  107,  112, 

115,  116,  118,  125-129 
Puebla  130-135 

Querretaro  216 

Salina  Cruz   159 

San  Andres  de  Tuxtla  246 

San  Angel  62,  67,  68 

San  Bartolito  74,  75 

San  Lsteban  59  —  61 

San  Juan  Teotihuacan  46—53 

San  Luis  Potosi  225 

Santa  Catarina  D.  F.  96 


Santiago  D.  F.  76 

Sierra  Mad  re  Oriental  230 

Sierra  Negra  (Puebla)   16 

Tacuba  58 

Tamasopo  Canon  231,233—237 

Taxco  174,175 

Tehuantepec  158,  160 

Teocelo   15 

Tepeapa  136 

Tepepam  80  —  83 

Tepozotlan  56,  57 

Tepoztlan  (Morelos)   167,170, 

171 
Tetzcoco  24 
Tetzcotzirgo  22 
Tlacopan  63 
Tlahuac  90 
TIalpam  D.  F    39 
Tlaxcala  23 
Toluca  212-215 
Tonilita  180 

Uruapam  202,  203 
Lxmal  252 

Photographs  of  Vegetation  6,  7, 
10  12,  17,  25,  40,41,69,76, 
77,84,93,  100,145,160,184, 
190, 208—211 .  215,231-237, 
240,  241,  247 

Vera  Cruz  3-5,  12 

Viga  Canal  86 

Photographs  of  Volcanoes  18, 
96—99,  116,  118,  125-129, 
178,  179,  181,  212,213 

Xicotepec  245 
Xochicalco   172,  173 
Xochimilco  87—89 

Zacatecas  223,  224 
Zapotitlan   142 
Zapotlan   181 


XIX 


Pico  de  Orizaba.     Estado  Puebla  Peak  of  Or.zaba.     State  of  Puebla 

Pic  von  Orizaba.    Staat  Puebla 
Piccod'Orizaba.    Stato  di  Puebla  Le  Pic  d  Orizaba,     fltat  de  Puebla 


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